Man And His Ancestor: A Study In EvolutionMorris, Charles
Science
Man And His Ancestor: A Study In Evolution
Morris, Charles
Human beings -- Origin
All geologists now believe that these accumulations were made by ice, at
some remote period when a very cold climate prevailed in the northern
hemisphere, and great glaciers slowly made their way southward, grinding
and rending as they went, and burying the land under their mountain-like
heaps, which sometimes were a mile or more in depth. In North America
the glacial ice pushed southward to the 40th degree of north latitude.
In Europe it extended to the Alpine region, but failed to reach the
countries bordering on the Mediterranean.
The elaborate and minute investigation of the glacial deposits has made
it highly probable that there were two glacial eras, two periods in
which the ice pushed down far to the south, and that these were
separated by a period in which the ice retreated and an age of warmer
weather intervened. This is known as the interglacial period. So far as
can be positively ascertained, all the authentic relics of man belong to
the Glacial Age. They seem first to become numerous in the interglacial
period, and continue to increase and become diversified as we descend
lower in time. How long ago it was that the sea of ice began its
downflow over the earth it is impossible to say. Some place it back six
hundred thousand or seven hundred thousand years. Some seek to bring it
down to a quite recent date. It is still so uncertain and such a matter
of controversy that the utmost we are able definitely to say is that it
was very long ago.
While there is no positive proof that men dwelt in Europe before the
coming on of the glacial chill, we have no just reason to doubt it. That
he lived there during glacial times is unquestionable, and we may be
very well assured that a naked tropical animal, destitute of the hairy
covering of the other animals, would not have chosen that frozen period
to migrate to the north. The fact that he was there during the ice age
seems satisfactory evidence that he was there before that age, during
the mild climate of late Tertiary times, and that--for a reason which we
shall hereafter consider--he was caught there and unable to retreat, and
was forced to adapt himself to the new conditions.
Public-domain text, read in full here on John Shaqi.
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